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<article article-type="research-article" dtd-version="1.3" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xml:lang="ru"><front><journal-meta><journal-id journal-id-type="publisher-id">hydrophysics</journal-id><journal-title-group><journal-title xml:lang="ru">Фундаментальная и прикладная гидрофизика</journal-title><trans-title-group xml:lang="en"><trans-title>Fundamental and Applied Hydrophysics</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2073-6673</issn><issn pub-type="epub">2782-5221</issn><publisher><publisher-name>St. Petersburg Research Center of the Russian Academy of Sciences</publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">hydrophysics-864</article-id><article-categories><subj-group subj-group-type="heading"><subject>Research Article</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>ФУНДАМЕНТАЛЬНЫЕ ВОПРОСЫ ГИДРОФИЗИКИ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>FUNDAMENTAL ISSUES OF HYDROPHYSICS</subject></subj-group></article-categories><title-group><article-title>Фронтальное столкновение внутренних волн большой амплитуды</article-title><trans-title-group xml:lang="en"><trans-title>Head-on Collision of Internal Waves of Large Amplitudes</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Мадерич</surname><given-names>В. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Maderich</surname><given-names>V. S.</given-names></name></name-alternatives><email xlink:type="simple">vladmad@gmail.com</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Терлецкая</surname><given-names>Е. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Terletska</surname><given-names>K. V.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Бровченко</surname><given-names>И. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Brovchenko</surname><given-names>I. A.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт проблем математических машин и систем Национальной академии наук Украины</institution><country>Россия</country></aff><aff xml:lang="en"><institution>The Institute of Mathematical Machines and Systems Problems of the Ukraine National Academy of Science (IMMSP NASU)</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2015</year></pub-date><pub-date pub-type="epub"><day>19</day><month>11</month><year>2022</year></pub-date><volume>8</volume><issue>3</issue><fpage>44</fpage><lpage>52</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Мадерич В.С., Терлецкая Е.В., Бровченко И.А., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Мадерич В.С., Терлецкая Е.В., Бровченко И.А.</copyright-holder><copyright-holder xml:lang="en">Maderich V.S., Terletska K.V., Brovchenko I.A.</copyright-holder><license xml:lang="ru" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>Данная работа распространяется под лицензией Creative Commons Attribution 4.0.</license-p></license><license xml:lang="en" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>This work is licensed under a Creative Commons Attribution 4.0 License.</license-p></license></permissions><self-uri xlink:href="https://hydrophysics.spbrc.ru/jour/article/view/864">https://hydrophysics.spbrc.ru/jour/article/view/864</self-uri><abstract><p>Численно исследуются динамика и энергетика фронтального столкновения уединенных внутренних волн большой амплитуды, распространяющихся в жидкости с двухслойной стратификацией. Расчеты проводятся в рамках уравнений Навье—Стокса в приближении Буссинеска. Показано, что в результате столкновения уединенных внутренних волн умеренных амплитуд возникает малый фазовый сдвиг и за прошедшими волнами генерируются дисперсионные цуги волн. Фазовый сдвиг растет с увеличением амплитуд взаимодействующих волн и при больших амплитудах приближается к предельному значению. При фронтальном столкновении волн больших амплитуд отклонение максимальной высоты от удвоенной амплитуды набегающих волн не увеличивается с их ростом, в отличие от волн умеренной амплитуды. Показано, что взаимодействие волн большой амплитуды приводит к сдвиговой неустойчивости и формированию вихрей Кельвина—Гельмгольца в слое раздела, однако затем волны снова становятся устойчивыми. </p></abstract><trans-abstract xml:lang="en"><p>The dynamics and energetics of a frontal collision of internal solitary waves of high amplitude propagating in a two-layer stratified fluid are studied numerically. The computations are carried out within the framework of the Navier—Stokes equations in the Boussinesq approximation. It was shown that the frontal collision of internal solitary waves of moderate amplitude leads to a small phase shift and to the generation of dispersive wavetrain trailing behind transmitted solitary wave. The phase shift grows with increasing amplitudes of the interacting waves and approaches the limiting value at large amplitudes of the waves. The deviation of the maximum wave height during collision from the twice the amplitude does not grow with increasing amplitude in the case of interaction of wave of large amplitude in contrast to the moderate amplitude waves. It was shown that the interaction of waves of large amplitude leads to the shear instability and the formation of Kelvin—Helmholtz vortices in the interface layer, however, subsequently waves again become stable. </p></trans-abstract><kwd-group xml:lang="ru"><kwd>внутренние волны большой амплитуды</kwd><kwd>численное моделирование</kwd><kwd>неустойчивость Кельвина—Гельмгольца</kwd></kwd-group><kwd-group xml:lang="en"><kwd>internal waves of large amplitude</kwd><kwd>numerical modelling</kwd><kwd>Kelvin—Helmholtz instability</kwd></kwd-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Grimshaw R., Pelinovsky E., Talipova T. Modeling internal solitary waves in the coastal ocean // Survey in Geophysics. 2007. № 28. P. 273—298.</mixed-citation><mixed-citation xml:lang="en">Grimshaw R., Pelinovsky E., Talipova T. Modeling internal solitary waves in the coastal ocean. 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